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Tenguyama Lava
- Volcanic rocks
- Pleistocene
- Lithofacies: Biotite hypersthene augite hornblende dacite lava
- Source: south of Murododaira
- Thickness: ca. 100 m
- Lower limit: Unconformity (Kunimidake Lava)
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Mount Tengu, Mount Tateyama, Toyama pref.
- Nakano et al. (2010) Jour. Geol. Soc. Japan, vol.116, Supplement, pp.37-48 DOI
- Harayama et al. (2000) Geology of the Tateyama District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 218p. (in Japanese with English abstract 6p.)